The Pacific Plate......
because it lies on a hotspot inside the pacific plate
The Antarctic plate is the tectonic plate that the continent of Antarctic. There are no countries on the Antarctic Plate.
Plate Tectonics. Plate Tectonics are the sub-layers that lie underneath the Earth's surface. They can rub against together, smash together, or pull away from each other. This is what caused Pangaea to separate.
With Plate Tectonics, Palawan lies more central to the Sunda plate than the rest of the Philippines. The rest of the Philippine Islands lie in the tectonically active area between the Philippine Sea Plate and the Sunda Plate. The islands were formed by Orogeny with the two plates colliding. Earthquakes in Palawan are said to be very few moderate sized earthquakes (due to not being on a plate boundary). See Wikipedia Links
Ridge push is a proposed mechanism for plate motion in plate tectonics. Because mid-ocean ridges lie at a higher elevation than the rest of the ocean floor, gravity causes the ridge to push on the lithosphere that lies farther from the ridge.Slab Pull is is tectonic plate motion due to higher densities. Plate motion is partly driven by the weight of cold, dense plates sinking into the mantle at trenches.
pacific and Australian
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it does not lie on a plte boundary but near the pacific plate
Pacific plate is the answer.
Alaska, Washington, Oregon, California, and Hawaii.
The boundary is between the Australian Plate and the Pacific Plate.
In the United States , the risk is highest along the Pacific coast in California, Washington, and Alaska. Plates meet along the Pacific coast, causing many active faults. In California , the Pacific plate and North American plate meet along the San Andreas fault. In Washington, earthquakes result from the subduction of the Juan de Fuca plate beneath the North American plate. In Alaska , subduction of the Pacific plate causes many earthquakes. The eastern United States generally has a low risk of earthquakes because this region lies far from plate boundaries. But , the East has experienced some of the most powerful quakes in the nation's history. Scientist hypothesize that the continental plate forming most of North America is under stress. This stress could disturb faults that lie hidden beneath thick layers of soil and rock.
In the United States , the risk is highest along the Pacific coast in California, Washington, and Alaska. Plates meet along the Pacific coast, causing many active faults. In California , the Pacific plate and North American plate meet along the San Andreas fault. In Washington, earthquakes result from the subduction of the Juan de Fuca plate beneath the North American plate. In Alaska , subduction of the Pacific plate causes many earthquakes. The eastern United States generally has a low risk of earthquakes because this region lies far from plate boundaries. But , the East has experienced some of the most powerful quakes in the nation's history. Scientist hypothesize that the continental plate forming most of North America is under stress. This stress could disturb faults that lie hidden beneath thick layers of soil and rock.
The boundary between the Gorda plate and the North American Plate is a transform boundary. Transform boundaries that lie at near land are the most destructive, which is the case in Southern California, which is close to this plate boundary.
There are two: Baja California (Statehood 1953) and Baja California Sur (Statehood 1974)
because it lies on a hotspot inside the pacific plate
Most volcanic eruptions occur in subduction zones, areas where crust is being drawn under the edge of a less dense plate, as in the Ring of Fire, a subduction zone around the Pacific Rim.